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Haliyal Taluk Uttarakannada District, Karnataka

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कᴂद्रीय भूमि जल बो셍ड जल संसाधन, नदी विकास और गंगा संरक्षण विभाग, जल शक्ति मंत्रालय भारत सरकार Central Ground Water Board Department of Water Resources, River Development and Ganga Rejuvenation, Ministry of Jal Shakti Government of India AQUIFER MAPPING AND MANAGEMENT OF GROUND WATER RESOURCES HALIYAL TALUK UTTARAKANNADA DISTRICT, KARNATAKA दवक्षण पविमी क्षेत्र, बℂगलोर South Western Region, Bengaluru FOR OFFICIAL USE ONLY RP/NAQUIM/2019-20/80 GOVERNMENT OF INDIA MINISTRY OF JAL SHAKTI DEPT. OF WATER RESOURCES, RD & GR CENTRAL GROUND WATER BOARD AQUIFER MANAGEMENT PLAN OF HALIYAL TALUK UTTARAKANNADA DISTRICT, KARNATAKA STATE By A. SURESHA Scientist ‘D’ STATE UNIT OFFICE BELGAUM April 2020 AQUIFER MANAGEMENT PLAN OF HALIYAL TALUK UTTARAKANNADA DISTRICT, KARNATAKA STATE CONTENTS Sl. No. Title Page No. 1 Salient information 1 2 Aquifer disposition 6 Ground water resource, extraction, Contamination and 3 8 other issues 4 Summary 11 AQUIFER MANAGEMENT PLAN OF HALIYAL TALUK, UTTARAKANNADA DISTRICT, KARNATAKA STATE 1.0 SALIENT INFORMATION Name of the taluk: Haliyal District: Uttarakannada; State: Karnataka Area: 847.45 sq.km. Population: 171426 Annual Normal Rainfall: 1328 mm 1.1 Aquifer management study area Aquifer mapping studies have been carried out in Haliyal taluk, Uttarakannada district of Karnataka, covering an area of 847.45 sq.kms under National Aquifer Mapping Project. Haliyal taluk of Uttarakannada district is located between North Latitudes 15°25’31’’ and 15°04’36.99” and East Longitudes between 74° 34’ 0.84” to 74° 54’38.88” and is falling in Survey of India Toposheets No forms parts of 48I/11, 48I/12, 48I/15 & 48I/16. The study area is bounded on the North by Khanapur taluk of Belagavi district, on the East by Dharwad district, on the South by Yellapur taluk and on west by Joida taluk of Uttarakannada district. Location map of Haliyal taluk of Uttarakannada district is presented in Fig-1. Haliyal is taluk headquarter and there are two towns, 24 grama panchayats, 4 hoblis and there are 110 villages in the taluk. Fig-1: Location map of Haliyal taluk of Uttarakannada district 1.2 Population According to 2011 census, the population in Haliyal taluk is 171426. Out of which 86601 are male while 84625 are females. The average sex ratio of Haliyal taluk is 975. The Haliyal taluk 1 has an overall population density of 202 persons per sq.km. The decadal growth rate in population from 2001-2011 is 7.72% in Haliyal taluk. 1.3 Rainfall The normal annual rainfall in Haliyal taluk for the period 1951 to 2000 is 1328 mm. The rainfall received show wide variation seasonally and major share of the annual precipitation is received from southwest monsoon, which is active during June-September months. The Southwest monsoon accounts for 85% of annual rainfall, whereas the winter rainfall contributes about 8 to 10%. The balance is received during pre monsoon period. The actual rainfall for the period from 2007 to 2017 is given in Table -1. Table –1: Actual rainfall (mm) for the period from 2007 to 2017 Year 2007 2008 2009 2010 2011 2012 2013 2014 2015 2016 2017 Rainfall 1403 1190 1472 1260 1492 924 1162 1326 863 871 1115 1.4 Agriculture & Irrigation Agriculture is the main occupation in Haliyal taluk. Major Kharif crops are Maize, Paddy and Vegetables. Main crops of Rabi season are paddy, vegetable and sugarcane (Table-2). Water intensive crops like sugarcane and paddy are grown in 70% of total crop area. Maize is grown in 18% and pulses in 3 % of total crop area of taluk. Cotton account for 4% and fruits & vegetables also account for 4% of total crop area. Table-2: Cropping pattern in Haliyal taluk 2017-18 (Ha) Fruits Maize Jowar Paddy Pulses Cotton Year Oil seedsOil Vegetables Sugarcane Area under cultivation (in ha) 2017-2018 3948 8935 2 758 774 32 9 6409 899 Source: District at a glance 2017-18, Govt. of Karnataka It is observed that net sown area accounts 25% and area sown more than once is 1.5 % of total geographical area in Haliyal taluk (Table-3) and shown in Fig.2. Area not available for cultivation and Fallow land cover 6 % & 1 % of total geographical area respectively. Forest area comprises about 68% total geographic area. Irrigation from bore well accounts for about 65.6% of the total area irrigated whereas irrigation from tanks accounts for 32.6% of the total area of irrigation. (Table-4). 2 Table-3: Details of land use in Haliyal taluk 2016-2017 (Ha) Area not Uncultiva Total Area Net Area sown available ble waste Fallow Taluk Geographical under sown more than for land land Area Forest area once cultivation Haliyal 84745 57819 3964 883 574 21505 1259 Source: District at a glance 2017-18, Govt. of Karnataka Fig-2: Land use Map Table 4: Irrigation details in Haliyal taluk (in ha) Numbers Net area irrigated % of area Source of Irrigation (Ha.) Canals nil Tanks 352 2529 32.65 Wells 6 nil Bore wells 1763 5082 65.6 Lift Irrigation nil Other Sources 134 1.7 Total 7745 Source: District at a glance 2017-18, Govt. of Karnataka 1.5 Geomorphology, Physiography & Drainage Haliyal taluk is a plain region formed by schistose formation. The central and southern parts exhibit moderate to gently “undulating terrain” having sparsely distributed knolls and tors. The remaining part of the taluk is in general a “plateau area”. This has its bearing on the regional slope which is towards northeast. The differential altitude is significant because, it is 3 likely to cause irregular ground water flow patterns on the micro scale (Fig. 3). Topography is dominantly controlled by geological structures. The entire area of Halyal taluka is being drained by Kali river and its tributaries. Generally, the drainage pattern of the river is dendritic to sub dendritic (Fig. 4). Fig-3: Geomorphology Map Fig-4: Drainage Map 1.6 Soil The soils of Haliyal taluk can broadly be classified into clayey and clayey skeletal soils. The clayey soils are produced in high rainfall area because of the leaching process. These soils vary in depth and texture, depending on the parent rock type, physiographic settings and climatic conditions (Fig. 5). 4 Fig-5: Soil Map 1.7 Ground water resource availability and extraction Aquifer wise total groundwater resources up to 200 m depth is given in Table-5 below. Table-5: Total Ground Water Resources (2013) (Ham) Taluk Annual replenishable Fresh In-storage GW Total availability of fresh GW resources resources GW resources Phreatic Fractured Dynamic + (Down to phreatic in-storage + HALIYAL 4215 200m) fractured 11970 3672 19857 1.8 Existing and future water demands (as per GEC-2017) Net ground water availability for future irrigation development : 45.12 MCM Domestic (Industrial sector) demand for next 25 years : 8.2 MCM 1.9 Water level behavior (a) Depth to water level Aquifer - I Pre-monsoon: 1.59 – 12.65 mbgl (Fig.6) Post-monsoon: 0.80 – 1.50 mbgl (Fig.7) (b) Water level fluctuation Aquifer-I (Fig.8) Seasonal Fluctuation: Rise ranges 0.74 – 11.85 m 5 Fig-6: Pre-monsoon Depth to Water Level (Aq-I) Fig-7: Post-monsoon Depth to Water Level (Aq-I) Fig-8: Water Level Fluctuation (Aq-I) 6 2.0 AQUIFER DISPOSITION 2.1 Number of aquifers: In Haliyal taluk, there are mainly two types of aquifer systems; i. Aquifer-I (Phreatic aquifer) Weathered schist ii. Aquifer-II (Fractured aquifer) Fractured schist In Haliyal taluk, schistose rocks of Dharwar group are the main water bearing formations (Fig- 9). Ground water occurs within the weathered and fractured schist under water table condition and semi-confined condition. In Haliyal taluk bore wells were drilled from a minimum depth of 181 mbgl to a maximum of 200 mbgl. Depth of weathered zone ranges from 7 to 10 mbgl. Ground water exploration reveals that aquifer-II fractured formation was encountered between the depth of 20 to 105 mbgl. Yield ranges from 0.20 to 5.5 lps. Ground water exploration done in this taluk is given in Table 5, and the basic characteristics of each aquifer are summarized in Table 6. Table-6: Details of Ground Water Exploration Sl. Location Lat/Long Depth Aquifer Discharg DTW DD T No Drilled/ Zones e m bgl (m) m2/day casing m.bgl (lpm) m bgl 1. Janaga- 15°14’ 14’’ 180.95/ 11.15 0.01 7.36 - - EW 74°49’ 53’’ 7.0 12.15 2. Kelagina- 15°15’ 15’’ 200.00/ 10.12 6.0 7.64 2.57 Koppa-EW 74°48’ 53’’ 12.20 12.5-16.2 Slug test 52.8-54.8 3. Havagi-EW 15°21’ 10’’ 200.00/1 10.5 305.4 3.22 23.70 11.115 74°45’ 08’’ 0.50 11.1-13.2 (APT) 29.4-30.4 49-49.8 69-72 83 102.6-103 Table-7: Basic characteristics of each aquifer Weathered Zone Aquifers Fractured Zone (Aquifer II) (Aquifer I) Prominent Lithology Weathered schist Fractured / Jointed schist Thickness range (mbgl) 20 Fractures upto 105 mbgl Depth range of occurrence of fractures (mbgl) 10-15 20-103 Range of yield potential (lps) Poor yield 1 - 5 2 T (m /day) - 2.5 – 11.0 Quality Suitability for Domestic &Irrigation Suitable Suitable 7 Fig-9: Geology Map 3.0 GROUND WATER RESOURCE, EXTRACTION, CONTAMINATION AND OTHER ISSUES 3.1 Aquifer wise resource availability and extraction Table 8 (a): Present Dynamic Ground Water Resource (2017) y lability For lability Taluk Net Annual Availabilit Water Ground Draft Existing Water Gross Ground For Irrigation Draft Existing Water Gross Ground Water For Domestic Industrial And Supply Draft Existing Water Gross Ground For All Uses Domestic Industrial Allocation And For Use25 Years For Next Net Avai GroundWater FutureIrrigation Development Water Existing Stage Of Ground Development Category Haliyal 4215 3037 76 3114 82 1096 74 Semicritical Table 8 (b): Present total Ground Water Resource (in ham) Taluk
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    Bull. Org. mond. Sante Bull. World Hlth Org.J 1951, 4, 75-109 SPREAD OF PLAGUE IN THE SOUTHERN AND CENTRAL DIVISIONS OF BOMBAY PROVINCE AND PLAGUE ENDEMIC CENTRES IN THE INDO-PAKISTAN SUBCONTINENT a M. SHARIF, D.Sc., Ph.D., F.N.I. Formerly Assistant Director in Charge of Department of Entomology, Haffkine Institute, Bombay b Manuscript received in September 1949 The findings of the Plague Recrudescence Inquiry in Sholapur and Adjoining Districts, conducted by Sharif & Narasimham11 12 in the districts of Sholapur and Dharwar during 1940 to 1943, do not support the idea that wild rodents help to carry plague infection from one place to another as in " temperate climes ".4 Wild rodents cannot be considered responsible for plague in Bombay Province, though they have been shown to be so in Transbaikalia, Mongolia, South-Eastern Russia, South Africa, and the western parts of the USA.17 In Bombay Province, the domestic rat perpetuates the plague infection. In some suitable places the infection among domestic rats goes on throughout the year. The infection is not apparent during the hot and dry season, its intensity being diminished because of the ill effect of prevailing climatic conditions on the wanderings of adult rat-fleas ; it pursues the course of a slow subterranean enzootic from burrow to burrow. The conclusion of the off-season is characterized by the advent of the rainy season, which exerts its influence in two ways first, it causes the rats from outside shelters to herd into burrows indoors and remain there perforce, which results in a considerable increase in the rat population within houses; secondly, it brings down the temperature and increases the humidity to such an extent as to result in a striking rise in the flea population and to allow rat-fleas to come out of burrows to attack human beings.
  • 0 0 23 Feb 2021 152000417

    0 0 23 Feb 2021 152000417

    Annexure I Annexure II ' .!'r ' .tu." "ffi* Government of Maharashtra, Directorate of Geology and Mining, "Khanij Bhavan",27, Shivaji Nagar, Cement Road, Nagpur-,1.10010 CERTIFICATE This is hereby certified that the mining lease granted to ]Ws Minerals & Metals over an area 27.45.20 Hec. situated in village Redi, Taluka Vengurla, District- Sindhudurg has no production of mineral since its originally lease deed execution. This certificate is issued on the basis of data provided by the District Collectorate, Sindhudurg. Mr*t, Place - Nagpur Director, Date - l1109/2020 Directorate of Geology and Mining, Government of Maharashtra, Nagpur 'ffi & r6nrr arn;r \k{rc sTrnrr qfrT6{ rtqailEc, ttufrg Qs, rr+at', fula rl-c, ffi qm, - YXo oqo ({lrr{ fF. osRe-?eao\e\\ t-m f. oeit-tlqqeqr f-+d , [email protected], [email protected]!.in *-.(rffi rw+m-12,S-s{r.r- x/?ol./ 26 5 5 flfii6- tocteo?o yfr, ll lsepzolo ifuflRirrs+ew, I J 1r.3TrvfdNfu{-{r rrs. \ffi-xooolq fus-q ti.H m.ffi, tu.frgq,l ffi ql* 1s.yr t ffiTq sF<-qrartq-qrsrufl -srd-d.. vs1{ cl fu€I EFro.{ srfffi, feqi,t fi q* fr.qo7o1,7qoqo. rl enqd qx fl<ato lq/os/?o?o Bq-tn Bqqri' gr{d,rr+ f frflw oTu-s +.€, r}.t* ar.ffi, fii.fufli ++d sll tir.xq t E'fr-qrqr T6 c$ Efurqgr tTer<ir+ RctsTcr{r :-err+ grd ;RrerrqTEkT squrq-d qT€t{d df,r{ +'t"qra *a eG. Tr6qrl :- irftf,fclo} In@r- t qr.{qrroi* qrqi;dqrf,q I fc.vfi.firqr|.